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《Journal of the Graduate School of the Chinese Academy of Science》 1997-01
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Tectonic and Sedimentary Evolution of the Xigaze Remnant-Type Forearc Basin

Hao Jie Li Yuejun (Institute of Geology,Academia Sinica,Beijing 100029)  
Xigaze Group, which developed in the Xigaze forearc basin between Gangdise Granites and Tsangpo Ophiolite in the Himalayan Orogenic Belt. was deposited on Tsangpo Ophiolite at the southern part of the basin, and was deposited on Gangdise Granites at the northern margin of the basin. We think that the southern basement and fore-ridge of the basin was composed of the Tsangpo super-subduction zone ophiolite, so the basin is classed under the Remnant-type forearc basin. During the early period of formation of the basin (K13), the ophiolitifeous slide deposit and radiolarian chert were developed in the basin, the sedimenst came from the fore-rigde; During the middle period (K21), the turbidite fan was well developed in the basin, the sediments came mainly from the northern Gangdise Arc; During the late period (K22-E2) - the basin evolved into littoral environment, and terrestrial deposit was developed in the northern margin of the basin and sorthen side of the fore-ridge. The collision between Indian Plate and Asian Plate probably occurred in Oligocene.
【Fund】: 中国科学院地质研究所所长基金支持课题
【CateGory Index】: P544.4
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